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Aspectos tafonômicos e o Efeito Lilliput em discinoideos do Devoniano da Bacia do Paraná, Sub-bacia Apucarana, Brasil

2016; UNIVERSIDADE DO VALE DO RIO DOS SINOS; Volume: 9; Issue: 1 Linguagem: Inglês

10.4013/gaea.2016.91.05

1983-3628

Jeanninny Carla Comniskey, Elvio Pinto Bosetti, Rodrigo Scalise Horodyski,

Geochemistry and Geologic Mapping

Discinoids are exclusively marine, epibenthic, inarticulate brachiopods, which use their pedicle to attach to the substrate. The global stratigraphic range of the genera range from the ?Ordovician to Holocene, but the Devonian period was the climax of this group. They have a broad geographical distribution and, in Brazil, are found in the Parana, Amazonas, Parnaiba and Parecis basins. The discinoids from the Parana Basin are found in the Ponta Grossa and Sao Domingos formations. Three genera of discinoids are recorded in the Brazilian Devonian strata, Orbiculoidea, Gigadiscina and Rugadiscina . Five species are recognized in the Parana basin ( Orbiculoidea baini, Orbiculoidea bodenbenderi, Orbiculoidea excentrica, Gigadiscina collis and Rugadiscina sp.). As far the taphonomy is concerned, the discinoids can be found isolated or in clusters, as complete and articulated valves, or as complete and disarticulated valves and/or fragmented valves, and constitute assemblages of shoreface and offshore settings. The analysis presented herein establishes the stratigraphic range of the Discinidae family between the late Pragian and the early Givetian. Orbiculoidea baini and Orbiculoidea excentrica showed phenotypes with reduced size attributed to the Lilliput Effect. This effect resulted of a biotic crisis recorded shortly before the collapse of Malvinokaffric fauna that caused a global extinction, the Kacak Event, in the Eifelian-Givetian transition. Keywords: Discinoids, Lilliput Effect, Devonian, Kacak Event, Taphonomy.